Changes in significant and maximum wave heights in the Norwegian Sea

This paper analyses 10years of in-situ measurements of significant wave height (Hs) and maximum wave height (Hmax) from the ocean weather ship Polarfront in the Norwegian Sea. The 30-minute Ship-Borne Wave Recorder measurements of Hmax and Hs are shown to be consistent with theoretical wave distribu...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Global and planetary change 2014-02, Vol.113, p.68-76
Hauptverfasser: Feng, Xiangbo, Tsimplis, M.N., Yelland, M.J., Quartly, G.D.
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 76
container_issue
container_start_page 68
container_title Global and planetary change
container_volume 113
creator Feng, Xiangbo
Tsimplis, M.N.
Yelland, M.J.
Quartly, G.D.
description This paper analyses 10years of in-situ measurements of significant wave height (Hs) and maximum wave height (Hmax) from the ocean weather ship Polarfront in the Norwegian Sea. The 30-minute Ship-Borne Wave Recorder measurements of Hmax and Hs are shown to be consistent with theoretical wave distributions. The linear regression between Hmax and Hs has a slope of 1.53. Neither Hs nor Hmax show a significant trend in the period 2000–2009. These data are combined with earlier observations. The long-term trend over the period 1980–2009 in annual Hs is 2.72±0.88cm/year. Mean Hs and Hmax are both correlated with the North Atlantic Oscillation (NAO) index during winter. The correlation with the NAO index is highest for the more frequently encountered (75th percentile) wave heights. The wave field variability associated with the NAO index is reconstructed using a 500-year NAO index record. Hs and Hmax are found to vary by up to 1.42m and 3.10m respectively over the 500-year period. Trends in all 30-year segments of the reconstructed wave field are lower than the trend in the observations during 1980–2009. The NAO index does not change significantly in 21st century projections from CMIP5 climate models under scenario RCP85, and thus no NAO-related changes are expected in the mean and extreme wave fields of the Norwegian Sea. •Hmax observed by SBWR is statistically consistent with theories.•The non-extreme wave fields are associated with the NAO.•NAO-related wave fields in past 500 and next 100years are assessed.
doi_str_mv 10.1016/j.gloplacha.2013.12.010
format Article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_1642217116</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><els_id>S0921818113002816</els_id><sourcerecordid>1642217116</sourcerecordid><originalsourceid>FETCH-LOGICAL-a483t-51031ef15276d13ae3ce52a3e5e6f584f4c9bbe5a2708af33d305777e895da803</originalsourceid><addsrcrecordid>eNqNkE1v1DAURS1UJKalv6HZIHWT4GfHH1lW0xaQKlgAa-vVeUk8SpzBzrTw70mZqtuyuptz75UOYxfAK-CgP-6qfpz3I_oBK8FBViAqDvwN24A1otRS1ydswxsBpQUL79hpzjvOwXAhNux6O2DsKRchFjn0MXTBY1wKjG0x4e8wHabiER-oGCj0w_KPWwYqvs7pkfqAsfhO-J697XDMdP6cZ-zn7c2P7efy7tunL9uruxJrK5dSAZdAHShhdAsSSXpSAiUp0p2ydVf75v6eFArDLXZStpIrYwzZRrVouTxjl8fdfZp_HSgvbgrZ0zhipPmQHehaCDAA-j9QYRqtRW1W1BxRn-acE3Vun8KE6Y8D7p4Uu517UeyeFDsQblW8Nj88n2D2OHYJow_5pS6sBKt4s3JXR45WOQ-Bkss-UPTUhkR-ce0cXv36C8iIlGQ</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1627966247</pqid></control><display><type>article</type><title>Changes in significant and maximum wave heights in the Norwegian Sea</title><source>Access via ScienceDirect (Elsevier)</source><creator>Feng, Xiangbo ; Tsimplis, M.N. ; Yelland, M.J. ; Quartly, G.D.</creator><creatorcontrib>Feng, Xiangbo ; Tsimplis, M.N. ; Yelland, M.J. ; Quartly, G.D.</creatorcontrib><description>This paper analyses 10years of in-situ measurements of significant wave height (Hs) and maximum wave height (Hmax) from the ocean weather ship Polarfront in the Norwegian Sea. The 30-minute Ship-Borne Wave Recorder measurements of Hmax and Hs are shown to be consistent with theoretical wave distributions. The linear regression between Hmax and Hs has a slope of 1.53. Neither Hs nor Hmax show a significant trend in the period 2000–2009. These data are combined with earlier observations. The long-term trend over the period 1980–2009 in annual Hs is 2.72±0.88cm/year. Mean Hs and Hmax are both correlated with the North Atlantic Oscillation (NAO) index during winter. The correlation with the NAO index is highest for the more frequently encountered (75th percentile) wave heights. The wave field variability associated with the NAO index is reconstructed using a 500-year NAO index record. Hs and Hmax are found to vary by up to 1.42m and 3.10m respectively over the 500-year period. Trends in all 30-year segments of the reconstructed wave field are lower than the trend in the observations during 1980–2009. The NAO index does not change significantly in 21st century projections from CMIP5 climate models under scenario RCP85, and thus no NAO-related changes are expected in the mean and extreme wave fields of the Norwegian Sea. •Hmax observed by SBWR is statistically consistent with theories.•The non-extreme wave fields are associated with the NAO.•NAO-related wave fields in past 500 and next 100years are assessed.</description><identifier>ISSN: 0921-8181</identifier><identifier>EISSN: 1872-6364</identifier><identifier>DOI: 10.1016/j.gloplacha.2013.12.010</identifier><language>eng</language><publisher>Amsterdam: Elsevier B.V</publisher><subject>Climate models ; Climatology ; Correlation ; Earth, ocean, space ; Exact sciences and technology ; External geophysics ; Marine ; Maximum wave height ; NAO ; North Atlantic oscillation ; Norwegian Sea ; Physics of the oceans ; Regression ; Ship-Borne Wave Recorder ; Significant wave height ; Surface waves, tides and sea level. Seiches ; Trends ; Weather ; Winter</subject><ispartof>Global and planetary change, 2014-02, Vol.113, p.68-76</ispartof><rights>2013 Elsevier B.V.</rights><rights>2015 INIST-CNRS</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a483t-51031ef15276d13ae3ce52a3e5e6f584f4c9bbe5a2708af33d305777e895da803</citedby><cites>FETCH-LOGICAL-a483t-51031ef15276d13ae3ce52a3e5e6f584f4c9bbe5a2708af33d305777e895da803</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/j.gloplacha.2013.12.010$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,780,784,3550,27924,27925,45995</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&amp;idt=28318509$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Feng, Xiangbo</creatorcontrib><creatorcontrib>Tsimplis, M.N.</creatorcontrib><creatorcontrib>Yelland, M.J.</creatorcontrib><creatorcontrib>Quartly, G.D.</creatorcontrib><title>Changes in significant and maximum wave heights in the Norwegian Sea</title><title>Global and planetary change</title><description>This paper analyses 10years of in-situ measurements of significant wave height (Hs) and maximum wave height (Hmax) from the ocean weather ship Polarfront in the Norwegian Sea. The 30-minute Ship-Borne Wave Recorder measurements of Hmax and Hs are shown to be consistent with theoretical wave distributions. The linear regression between Hmax and Hs has a slope of 1.53. Neither Hs nor Hmax show a significant trend in the period 2000–2009. These data are combined with earlier observations. The long-term trend over the period 1980–2009 in annual Hs is 2.72±0.88cm/year. Mean Hs and Hmax are both correlated with the North Atlantic Oscillation (NAO) index during winter. The correlation with the NAO index is highest for the more frequently encountered (75th percentile) wave heights. The wave field variability associated with the NAO index is reconstructed using a 500-year NAO index record. Hs and Hmax are found to vary by up to 1.42m and 3.10m respectively over the 500-year period. Trends in all 30-year segments of the reconstructed wave field are lower than the trend in the observations during 1980–2009. The NAO index does not change significantly in 21st century projections from CMIP5 climate models under scenario RCP85, and thus no NAO-related changes are expected in the mean and extreme wave fields of the Norwegian Sea. •Hmax observed by SBWR is statistically consistent with theories.•The non-extreme wave fields are associated with the NAO.•NAO-related wave fields in past 500 and next 100years are assessed.</description><subject>Climate models</subject><subject>Climatology</subject><subject>Correlation</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Marine</subject><subject>Maximum wave height</subject><subject>NAO</subject><subject>North Atlantic oscillation</subject><subject>Norwegian Sea</subject><subject>Physics of the oceans</subject><subject>Regression</subject><subject>Ship-Borne Wave Recorder</subject><subject>Significant wave height</subject><subject>Surface waves, tides and sea level. Seiches</subject><subject>Trends</subject><subject>Weather</subject><subject>Winter</subject><issn>0921-8181</issn><issn>1872-6364</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2014</creationdate><recordtype>article</recordtype><recordid>eNqNkE1v1DAURS1UJKalv6HZIHWT4GfHH1lW0xaQKlgAa-vVeUk8SpzBzrTw70mZqtuyuptz75UOYxfAK-CgP-6qfpz3I_oBK8FBViAqDvwN24A1otRS1ydswxsBpQUL79hpzjvOwXAhNux6O2DsKRchFjn0MXTBY1wKjG0x4e8wHabiER-oGCj0w_KPWwYqvs7pkfqAsfhO-J697XDMdP6cZ-zn7c2P7efy7tunL9uruxJrK5dSAZdAHShhdAsSSXpSAiUp0p2ydVf75v6eFArDLXZStpIrYwzZRrVouTxjl8fdfZp_HSgvbgrZ0zhipPmQHehaCDAA-j9QYRqtRW1W1BxRn-acE3Vun8KE6Y8D7p4Uu517UeyeFDsQblW8Nj88n2D2OHYJow_5pS6sBKt4s3JXR45WOQ-Bkss-UPTUhkR-ce0cXv36C8iIlGQ</recordid><startdate>20140201</startdate><enddate>20140201</enddate><creator>Feng, Xiangbo</creator><creator>Tsimplis, M.N.</creator><creator>Yelland, M.J.</creator><creator>Quartly, G.D.</creator><general>Elsevier B.V</general><general>Elsevier</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7TN</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H97</scope><scope>KL.</scope><scope>L.G</scope><scope>8FD</scope><scope>FR3</scope><scope>H8D</scope><scope>KR7</scope><scope>L7M</scope></search><sort><creationdate>20140201</creationdate><title>Changes in significant and maximum wave heights in the Norwegian Sea</title><author>Feng, Xiangbo ; Tsimplis, M.N. ; Yelland, M.J. ; Quartly, G.D.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a483t-51031ef15276d13ae3ce52a3e5e6f584f4c9bbe5a2708af33d305777e895da803</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2014</creationdate><topic>Climate models</topic><topic>Climatology</topic><topic>Correlation</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Marine</topic><topic>Maximum wave height</topic><topic>NAO</topic><topic>North Atlantic oscillation</topic><topic>Norwegian Sea</topic><topic>Physics of the oceans</topic><topic>Regression</topic><topic>Ship-Borne Wave Recorder</topic><topic>Significant wave height</topic><topic>Surface waves, tides and sea level. Seiches</topic><topic>Trends</topic><topic>Weather</topic><topic>Winter</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Feng, Xiangbo</creatorcontrib><creatorcontrib>Tsimplis, M.N.</creatorcontrib><creatorcontrib>Yelland, M.J.</creatorcontrib><creatorcontrib>Quartly, G.D.</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Meteorological &amp; Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 3: Aquatic Pollution &amp; Environmental Quality</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Civil Engineering Abstracts</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Global and planetary change</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Feng, Xiangbo</au><au>Tsimplis, M.N.</au><au>Yelland, M.J.</au><au>Quartly, G.D.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Changes in significant and maximum wave heights in the Norwegian Sea</atitle><jtitle>Global and planetary change</jtitle><date>2014-02-01</date><risdate>2014</risdate><volume>113</volume><spage>68</spage><epage>76</epage><pages>68-76</pages><issn>0921-8181</issn><eissn>1872-6364</eissn><abstract>This paper analyses 10years of in-situ measurements of significant wave height (Hs) and maximum wave height (Hmax) from the ocean weather ship Polarfront in the Norwegian Sea. The 30-minute Ship-Borne Wave Recorder measurements of Hmax and Hs are shown to be consistent with theoretical wave distributions. The linear regression between Hmax and Hs has a slope of 1.53. Neither Hs nor Hmax show a significant trend in the period 2000–2009. These data are combined with earlier observations. The long-term trend over the period 1980–2009 in annual Hs is 2.72±0.88cm/year. Mean Hs and Hmax are both correlated with the North Atlantic Oscillation (NAO) index during winter. The correlation with the NAO index is highest for the more frequently encountered (75th percentile) wave heights. The wave field variability associated with the NAO index is reconstructed using a 500-year NAO index record. Hs and Hmax are found to vary by up to 1.42m and 3.10m respectively over the 500-year period. Trends in all 30-year segments of the reconstructed wave field are lower than the trend in the observations during 1980–2009. The NAO index does not change significantly in 21st century projections from CMIP5 climate models under scenario RCP85, and thus no NAO-related changes are expected in the mean and extreme wave fields of the Norwegian Sea. •Hmax observed by SBWR is statistically consistent with theories.•The non-extreme wave fields are associated with the NAO.•NAO-related wave fields in past 500 and next 100years are assessed.</abstract><cop>Amsterdam</cop><pub>Elsevier B.V</pub><doi>10.1016/j.gloplacha.2013.12.010</doi><tpages>9</tpages><oa>free_for_read</oa></addata></record>
fulltext fulltext
identifier ISSN: 0921-8181
ispartof Global and planetary change, 2014-02, Vol.113, p.68-76
issn 0921-8181
1872-6364
language eng
recordid cdi_proquest_miscellaneous_1642217116
source Access via ScienceDirect (Elsevier)
subjects Climate models
Climatology
Correlation
Earth, ocean, space
Exact sciences and technology
External geophysics
Marine
Maximum wave height
NAO
North Atlantic oscillation
Norwegian Sea
Physics of the oceans
Regression
Ship-Borne Wave Recorder
Significant wave height
Surface waves, tides and sea level. Seiches
Trends
Weather
Winter
title Changes in significant and maximum wave heights in the Norwegian Sea
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-28T16%3A03%3A30IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Changes%20in%20significant%20and%20maximum%20wave%20heights%20in%20the%20Norwegian%20Sea&rft.jtitle=Global%20and%20planetary%20change&rft.au=Feng,%20Xiangbo&rft.date=2014-02-01&rft.volume=113&rft.spage=68&rft.epage=76&rft.pages=68-76&rft.issn=0921-8181&rft.eissn=1872-6364&rft_id=info:doi/10.1016/j.gloplacha.2013.12.010&rft_dat=%3Cproquest_cross%3E1642217116%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=1627966247&rft_id=info:pmid/&rft_els_id=S0921818113002816&rfr_iscdi=true